Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems
Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Doser, Diane I. [verfasserIn] |
|---|
| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014transfer abstract |
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| Umfang: |
9 |
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| Übergeordnetes Werk: |
Enthalten in: Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community - Borri, Maria ELSEVIER, 2020, international journal of geotectonics and the geology and physics of the interior of the earth, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:611 ; year:2014 ; day:25 ; month:01 ; pages:121-129 ; extent:9 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.tecto.2013.11.018 |
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ELV017197139 |
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| 520 | |a Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. | ||
| 520 | |a Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. | ||
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10.1016/j.tecto.2013.11.018 doi GBVA2014001000014.pica (DE-627)ELV017197139 (ELSEVIER)S0040-1951(13)00683-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.63 bkl Doser, Diane I. verfasserin aut Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:611 year:2014 day:25 month:01 pages:121-129 extent:9 https://doi.org/10.1016/j.tecto.2013.11.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 611 2014 25 0125 121-129 9 045F 550 |
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10.1016/j.tecto.2013.11.018 doi GBVA2014001000014.pica (DE-627)ELV017197139 (ELSEVIER)S0040-1951(13)00683-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.63 bkl Doser, Diane I. verfasserin aut Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:611 year:2014 day:25 month:01 pages:121-129 extent:9 https://doi.org/10.1016/j.tecto.2013.11.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 611 2014 25 0125 121-129 9 045F 550 |
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10.1016/j.tecto.2013.11.018 doi GBVA2014001000014.pica (DE-627)ELV017197139 (ELSEVIER)S0040-1951(13)00683-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.63 bkl Doser, Diane I. verfasserin aut Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:611 year:2014 day:25 month:01 pages:121-129 extent:9 https://doi.org/10.1016/j.tecto.2013.11.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 611 2014 25 0125 121-129 9 045F 550 |
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10.1016/j.tecto.2013.11.018 doi GBVA2014001000014.pica (DE-627)ELV017197139 (ELSEVIER)S0040-1951(13)00683-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.63 bkl Doser, Diane I. verfasserin aut Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:611 year:2014 day:25 month:01 pages:121-129 extent:9 https://doi.org/10.1016/j.tecto.2013.11.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 611 2014 25 0125 121-129 9 045F 550 |
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10.1016/j.tecto.2013.11.018 doi GBVA2014001000014.pica (DE-627)ELV017197139 (ELSEVIER)S0040-1951(13)00683-5 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.63 bkl Doser, Diane I. verfasserin aut Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems 2014transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. Enthalten in Elsevier Borri, Maria ELSEVIER Pediatric Adrenal Insufficiency - Quality Improvement from Clinic to Community 2020 international journal of geotectonics and the geology and physics of the interior of the earth Amsterdam [u.a.] (DE-627)ELV00416637X volume:611 year:2014 day:25 month:01 pages:121-129 extent:9 https://doi.org/10.1016/j.tecto.2013.11.018 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA 44.63 Krankenpflege VZ AR 611 2014 25 0125 121-129 9 045F 550 |
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seismicity of southwestern yukon, canada, and its relation to slip transfer between the fairweather and denali fault systems |
| title_auth |
Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems |
| abstract |
Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. |
| abstractGer |
Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. |
| abstract_unstemmed |
Several researchers have postulated the existence of a fault (termed the Connector fault) that transfers slip from the Fairweather to the Denali fault systems in order to match the observed regional variations in fault slip and GPS deformation. Earthquake locations, seismic moment tensor information, and gravity data presented in this study suggest that the Connector fault is an active seismogenic structure that extends from the Fairweather fault near Hubbard Glacier to the intersection of the Duke River and Totschunda fault systems. Seismicity and potential field data also suggest the existence of an east–west trending cross structure between the Totschunda and Denali faults just north of 62°N that appears to be taking up compressional deformation similar to the Duke River fault system to the south. The intersection of this cross structure with the Totschunda fault occurs near the termination of the 2002 Denali fault mainshock rupture zone. |
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Seismicity of Southwestern Yukon, Canada, and its relation to slip transfer between the Fairweather and Denali fault systems |
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https://doi.org/10.1016/j.tecto.2013.11.018 |
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